Comment on “Pore water flow due to near-bed turbulence and associated solute transfer in a stream or lake sediment bed” by M. Higashino et al.

Turbulence structure of open channel flows over permeable and impermeable beds: A comparative study

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Gravity-driven water exchange between streams and hyporheic zones

(2009) F. Boano et al.   GEOPHYSICAL RESEARCH LETTERS

Depth-Dependent Dispersion Coefficient for Modeling of Vertical Solute Exchange in a Lake Bed under Surface Waves

(2009) Qin Qian et al.   JOURNAL OF HYDRAULIC ENGINEERING

Modeling of Vertical Solute Dispersion in a Sediment Bed Enhanced by Wave-Induced Interstitial Flow

(2009) Qin Qian et al.   JOURNAL OF THE AMERICAN WATER RESOURCES ASSOCIATION

Pore water flow due to near-bed turbulence and associated solute transfer in a stream or lake sediment bed

(2009) Makoto Higashino et al.   WATER RESOURCES RESEARCH

A vertical dispersion model for solute exchange induced by underflow and periodic hyporheic flow in a stream gravel bed

(2008) Qin Qian et al.   WATER RESOURCES RESEARCH